Some Salient Points in the Science of the EarthDawson, John William, Sir
Science
Some Salient Points in the Science of the Earth
Dawson, John William, Sir
Geology; Paleontology
(6) Though the roots of _Sigillaria_ bear some resemblance to the
rhizomes of certain aquatic plants, yet structurally they have much
resemblance to the roots of Cycads, which the stems also resemble.
Further, the _Sigillariæ_ grew on the same soils which supported
conifers, _Lepidodendra_, _Cordaites_, and ferns, plants which could
not have grown in water. Again, with the exception, perhaps, of some
_Pinnulariæ_ and _Asterophyllites_, and Rhizocarpean spores, there is
a remarkable absence from the coal measures of any form of properly
aquatic vegetation.
(7) The occasional occurrence of marine or brackish-water animals in
the roofs of coal beds, or even in the coal itself, affords no evidence
of subaqueous accumulation, since the same thing occurs in the case of
modern submarine forests. Such facts merely imply that portions of the
areas of coal accumulation were liable to inundation of a character so
temporary as not finally to close the process, as happened when at last
a roof shale was deposited by water over the coal. Cannel coals and
bituminous shales holding mussel-like shells, fish scales, etc., imply
the existence sometimes for long periods of ponds, lakes or lagoons
in the coal swamps, but ordinary coal did not accumulate in these. It
is in the cannels and similar subaqueous coals that the macrospores
which I attribute in great part to aquatic plants, allied to modern
Salvinia, etc., are chiefly found.[115]
[115] "Geological History of Plants," _Bulletin Chicago Academy of
Sciences_, 1886.
For these and other reasons, some of which are more fully stated in the
papers referred to, while I admit that the areas of coal accumulation
were frequently submerged, I must maintain that the true coal is a
subaërial accumulation by vegetable growth on soils wet and swampy,
it is true, but not submerged. I would add the further consideration,
already urged elsewhere, that in the case of the fossil forests
associated with the coal, the conditions of submergence and silting-up
which have preserved the trees as fossils, must have been precisely
those which were fatal to their existence as living plants, a fact
sufficiently evident to us in the case of modern submarine forests, but
often overlooked by the framers of theories of the accumulation of coal.
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